CLIMATE CHANGE & CRITICAL RESOURCES. Iratxe González-Aparicio Tlfn:
|
|
- Conrad Jenkins
- 5 years ago
- Views:
Transcription
1 CLIMATE CHANGE & CRITICAL RESOURCES Iratxe González-Aparicio Tlfn:
2 OUTLINE 1. Introduction. IPCC last releases 2. Regional Models and Data 3. Scenarios of Climate Change in the Basque Region 4. Critical Resources Future Urban Atmosphere 5. Scenarios of the Urban Boundary Layer over Bilbao 6. Conclusions 7. Some Useful References
3 1. INTRODUCTION. IPCC last releases IPCC Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation Is climate change leading to increase in the number and severity of extreme events? How do social and environmental factors interact with weather and climate events to create disasters? What can be done to make societies more resilient to extremes? IPCC Assessment Reports: 1990, 1995, 2001 and 2007 The Fifth AR will appear in four stages in 2013 and 2014.
4 3. Regional Models and Data Escenarios Climáticos: Proyecto ENSEMBLES ENSEMBLES Características Escala Regional Resolución 25 km * 25 km Esc. Emisiones A1B Periodo de referencia Escenarios futuros //2100
5 3. Climate Change in the Basque Country 90th percentile of the Tmax Ensemble Av. 35.6ºC Spread:3.5ºC Stdv:1.41ºC Ensemble Av. 37.8ºC Spread:6.52ºC Stdv:2.54ºC Ensemble Av. 39.7ºC Spread: 4.6ºC Stdv:1.87ºC Future projection: trend: 3ºC Stdv ºC Spread: 4.2ºC
6 3. Climate Change in the Basque Country Heat Waves duration Obs. Av. 1.3 heat waves Freq: 13.7 days Temp: 29 ºC Ensembles Freq. 1-2 heat waves Av days [12%] Ensembles Freq. 1-2 heat waves Av days [16%] Ensembles Freq. 1-3 heat waves Av days [22%] Temp involved 34.7 ºC Temp involved 34.3 ºC Temp involved 34.2 ºC
7 3. Climate Change in the Basque Country 10th percentile Tmin Ensemble Av ºC Spread: 1.8ºC Stdv: 0.71ºC Ensemble Av ºC Spread: 1.72ºC Stdv:0.68ºC Ensemble Av ºC Spread:1.5ºC Stdv: 0.92ºC Future scenario: trend: 3ºC Stdv ºC Spread: 1.83ºC
8 3. Climate Change in the Basque Country Number of frost days Ensemble Av d Stdv: 3.5 d Ensemble Av d Stdv: 3.9 d Ensemble Av. 7.5 d Stdv: 3.57 d Future scenario ( ) Decrease 50% of days Respect with Ref. Period
9 3. Climate Change in the Basque Country Cold Waves duration Obs. Av cold waves Freq: 11.1 days [12%] Temp: 3.3 ºC Ensembles Freq. 1-3 cold waves Av days [14%] Ensembles Freq. 1-2 cold waves Av days [9%] RACMO/REMO/ALADIN Freq. 1 cold wave Av. 6-9 days [8%] HIRHAM/CLM/PROMES: 0 Temp involved 2.7 ºC Temp involved 3.3 ºC Temp involved 1.3ºC
10 3. Climate Change in the Basque Country Summer Winter
11
12 3. Climate Change in the Basque Country SUMMER Rise in the air mean temperature leading to enhance the kinetic energy of the gas-phase equilibrium: i.e. the capacity to hold water vapour in the air increases. Linked with the positive slope in the specific humidity. Income short-wave radiation expected a reduction decrease in the cloudiness decrease of the modelled precipitation. A slight decrease wind speed, no significant changes in wind direction. WINTER Solar radiation evolution indicated a decrease, more cloudiness more probability of rain. Rise air mean temperature increase specific humidity + water vapour Change of the specific humidity in winter greater than summer greater moisten atmosphere by higher temperatures and precipitations.
13 4. CRITICAL RESOURCES Urban Atmosphere
14
15 Winter: /24-29 January : Cold Summer air mass from July N-C 2009: Europe The air mass - Pressure swept Ridge into the Central Bilbao Europe valley from the S-E dir, pushed by - Anticliclonic a high pressure conditions ridge placed in the north of the - Temp: Great 21. Britain. 8ºC Strong winds, 11.4 ºC a southern - Diurnal warm sea breeze air mass blows was from transported NW-N-NE northward through the - Nocturnal Atlantic Ocean, valley breezes displacing from the the cold SE air masses to the south through Central Europe
16
17
18
19 GENERATION OF URBAN SCENARIOS FOR BILBAO Base de datos: UDALPLAN
20
21
22 6. General Conclusions Local Climate and Atmospheric Composition is affected by Regional Variability + Urban Development The Basque Country Region is affected by Climatic Change expecting a Worsen of Extreme Events. At present, in the Bilbao metropolitan area, under specific conditions, it appears critical situations enhancing the extreme meteo conditions and atmospheric compo. levels Under different urban scenarios, the Critical situations are Much more pronounced.
23 Some Additional References: González-Aparicio, I., Nuterman R., Korsholm U.S., Mahura A., Acero J.A., Hidalgo J. & Baklanov A. PROCESSING OF LAND-USE DATABASE FOR MESO-SCALE MODEL URBANIZATION. Newsletter 9, NL , p.9 González-Aparicio, I., Nuterman R., Korsholm U.S., Mahura A., Acero J.A., Hidalgo J. & Baklanov A. LAND-USE DATABASE PROCESSING APPROACH FOR MESO-SCALE URBAN NWP MODEL INITIALIZATION. DMI Scientific Report 10-02, 34 pages. ISBN: , 2010 Alexander Mahura, Roman Nuterman, Iratxe Gonzalez-Aparicio, Claus Petersen, Alexander Baklanov & Ulrik Korsholm. ENVIRONMENTAL MODELING IN METROPOLITAN AREAS. Scientific Report. DMI /In preparation/ Nuterman R., Baklanov A., Mahura A., Zakey A., Korsholm U., Bjarne A. & González-Aparicio I. MULTI-SCALE AIR QUALITY FORECAST: DOWNSCALING FROM REGIONAL TO STREET SCALE. Newsletter 9, NL , p.10 González- Aparicio I., Nuterman R., Korsholm U., Mahura A., Hidalgo J. & Baklanov A URBAN SCALE MODELLING FOR A MEGACITY AND A MEDIUM SIZE CITY: EVALUATING SULPHATE AEROSOL INDIRECT EFFECT. European Geoscience Union. General Assembly. AS3.6: Megacities: Air Quality and climate impacts from local to global scales. Vienna 3-8 April 2010.
24 Baklanov a, Korsholm U., Mahura A., Zakey A, Nuterman R, Sass B, Nielsen C, Kaas E, Sorensen B, Gonzalez-Aparicio I. Enviro-HIRLAM ONLINE INTEGRATED ACT-NWP MODELING SYSTEM WITH TWO-WAY INTERACTIONS: HISTORY AND CURRENT STATUS. European Geoscience Union. General Assembly. AS3.6: Megacities: Air Quality and climate impacts from local to global scales. Vienna 3-8 April Nuterman R, Baklanov A, Zakey A, Amstrup B, González-Aparicio I, Weisman J. MULTI-SCALE METEOROLOGICAL AND CHEMICAL WEATHER FORECASTING WITH DOWNSCALING MODEL SYSTEM. M Sofiev, M Prank, J Kukkonen, A Segers, P Builtjes, H D van der Gon, U Korsholm, I Gonzalez-Aparicio, R Nuterman, A Mahura, A Baklanov, S Pandis. EVALUATION AND IMPROVEMENT OF REGIONAL MODEL SIMULATIONS FOR MEGACITY PLUMES. MEGAPOLI Technical Note Helsinki, Mahura A, González-Aparicio I., Baklanov A., Evaluation of Environmental Pollution from Severonickel Plant, Kola Peninsula. Manuscript in prepatation for Meteorology and Hydrology journal. González-Aparicio, I. and Hidalgo, J. RECENT TEMPERATURE SCENARIOS FOR THE NORTHERN IBERIAN PENINSULA. A BIAS CORRECTION METHOD FOR CLIMATIC INDICES EXPRESSED IN A DAILY BASED FREQUENCY. International Journal of Climatology [Submitted]. 11th International Conference of Statistical Climatology. Oral presentation. July, 2010.
25 Thank you for your attention Iratxe González-Aparicio Tlfn:
Russian State Hydrometeorological University (RSHU), Russia 2
Georgy Nerobelov 1*, Margarita Sedeeva 1, Alexander Mahura 2, Roman Nuterman 3, Suleiman Mostamandi 1, Sergeii Smyshlyaev 1 1 Russian State Hydrometeorological University (RSHU), Russia 2 Institute for
More informationMarcoPolo. Monitoring and Assessment of Regional air quality in China using space Observations. Project Of Long-term sino-european co-operation
Project no. 606953 MarcoPolo Monitoring and Assessment of Regional air quality in China using space Observations. Project Of Long-term sino-european co-operation Type of funding scheme: Collaborative Project
More informationSPECIAL PROJECT PROGRESS REPORT
SPECIAL PROJECT PROGRESS REPORT Progress Reports should be 2 to 10 pages in length, depending on importance of the project. All the following mandatory information needs to be provided. Reporting Year:
More informationOther Presentations (at workshops/meetings/seminars/ ) & Publications (in journals/newsletters/ )
Other Presentations (at workshops/meetings/seminars/ ) & Publications (in journals/newsletters/ ) 1. (2016) Mahura A., R. Nuterman, K.P. Nielsen, X. Yang, B. Amstrup, A. Baklanov (2016): Regional Subregional
More informationNorthern New England Climate: Past, Present, and Future. Basic Concepts
Northern New England Climate: Past, Present, and Future Basic Concepts Weather instantaneous or synoptic measurements Climate time / space average Weather - the state of the air and atmosphere at a particular
More informationExtremes Events in Climate Change Projections Jana Sillmann
Extremes Events in Climate Change Projections Jana Sillmann Max Planck Institute for Meteorology International Max Planck Research School on Earth System Modeling Temperature distribution IPCC (2001) Outline
More informationEuropean Developments in Mesoscale Modelling for Air Pollution Applications Activities of the COST 728 Action
European Developments in Mesoscale Modelling for Air Pollution Applications Activities of the COST 728 Action R S Sokhi*, A Baklanov, H Schlünzen, M Sofiev, M Athanassiadou, Peter Builtjes and COST 728
More informationDownscaled Climate Change Projection for the Department of Energy s Savannah River Site
Downscaled Climate Change Projection for the Department of Energy s Savannah River Site Carolinas Climate Resilience Conference Charlotte, North Carolina: April 29 th, 2014 David Werth Atmospheric Technologies
More informationClimate changes in Finland, but how? Jouni Räisänen Department of Physics, University of Helsinki
Climate changes in Finland, but how? Jouni Räisänen Department of Physics, University of Helsinki 19.9.2012 Outline Some basic questions and answers about climate change How are projections of climate
More informationObserved State of the Global Climate
WMO Observed State of the Global Climate Jerry Lengoasa WMO June 2013 WMO Observations of Changes of the physical state of the climate ESSENTIAL CLIMATE VARIABLES OCEANIC ATMOSPHERIC TERRESTRIAL Surface
More informationRegional Climate Simulations with WRF Model
WDS'3 Proceedings of Contributed Papers, Part III, 8 84, 23. ISBN 978-8-737852-8 MATFYZPRESS Regional Climate Simulations with WRF Model J. Karlický Charles University in Prague, Faculty of Mathematics
More informationRoad Weather Modelling System: Verification for Road Weather Season
Road Weather Modelling System: Verification for 2009-2010 Road Weather Season Claus Petersen, Alexander Mahura, Bent Sass Copenhagen 2010 www.dmi.dk/dmi/tr10-12.pdf page 1 of 20 Colophon Serial title:
More informationClimate Dataset: Aitik Closure Project. November 28 th & 29 th, 2018
1 Climate Dataset: Aitik Closure Project November 28 th & 29 th, 2018 Climate Dataset: Aitik Closure Project 2 Early in the Closure Project, consensus was reached to assemble a long-term daily climate
More informationScientific/ Technical Reports &Contributions to Reports
Scientific/ Technical Reports &Contributions to Reports 1. (2015) Stysiak A., Bergen M.J., Mahura A. (2015): Impact of regional afforestation on climatic conditions in Copenhagen Metropolitan Area. DMI
More informationTechnical Report Road Weather Modelling System: Verification for Road Weather Season. Claus Petersen, Alexander Mahura, Bent Sass
Technical Report 09-10 Road Weather Modelling System: Verification for 2008-2009 Road Weather Season Claus Petersen, Alexander Mahura, Bent Sass www.dmi.dk/dmi/tr09-10 Copenhagen 2009 page 1 of 20 Colophon
More informationValidation of 2-meters temperature forecast at cold observed conditions by different NWP models
Validation of 2-meters temperature forecast at cold observed conditions by different NWP models Evgeny Atlaskin Finnish Meteorological Institute / Russian State Hydrometeorological University OUTLINE Background
More informationAnnex I to Target Area Assessments
Baltic Challenges and Chances for local and regional development generated by Climate Change Annex I to Target Area Assessments Climate Change Support Material (Climate Change Scenarios) SWEDEN September
More informationRoad Weather Modelling System: Verification for Road Weather Season
Road Weather Modelling System: Verification for 2007-2008 Road Weather Season Claus Petersen, Alexander Mahura, Bent Sass, Torben Pedersen Copenhagen 2008 www.dmi.dk/dmi/tr08-09 page 1 of 14 Colophon Serial
More informationScience 1206 Weather Unit REVIEW Short Answer
Science 1206 Weather Unit REVIEW Short Answer 1. Which is defined as the short-term conditions of the atmosphere? 2. Which is defined as the long-term conditions of the atmosphere? 3. Which is used to
More informationClimate Projections and Energy Security
NOAA Research Earth System Research Laboratory Physical Sciences Division Climate Projections and Energy Security Andy Hoell and Jim Wilczak Research Meteorologists, Physical Sciences Division 7 June 2016
More informationATM S 111, Global Warming Climate Models
ATM S 111, Global Warming Climate Models Jennifer Fletcher Day 27: July 29, 2010 Using Climate Models to Build Understanding Often climate models are thought of as forecast tools (what s the climate going
More informationClimate variability and the expected. Croatia
Climate variability and the expected effects of climate change scenario in Croatia Krešo Pandžić Meteorological and Hydrological Service Croatia National roundtable Adaptation to climate change, Zagreb,
More informationREQUEST FOR A SPECIAL PROJECT
REQUEST FOR A SPECIAL PROJECT 2013 2015 MEMBER STATE: Denmark.... Principal Investigator 1 : Affiliation: Address: E-mail: Other researchers: Project Title: Prof., Dr. Alexander Baklanov. Danish Meteorological
More information8th EMS Annual Meeting and 7th European Conference on Applied Climatology 2008
Adv. Sci. Res., 3, 53 57, 2009 Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Multi-scale atmospheric environment modelling for urban areas A. A. Baklanov
More informationPERFORMANCE OF THE WRF-ARW IN THE COMPLEX TERRAIN OF SALT LAKE CITY
P2.17 PERFORMANCE OF THE WRF-ARW IN THE COMPLEX TERRAIN OF SALT LAKE CITY Jeffrey E. Passner U.S. Army Research Laboratory White Sands Missile Range, New Mexico 1. INTRODUCTION The Army Research Laboratory
More informationOperational event attribution
Operational event attribution Peter Stott, NCAR, 26 January, 2009 August 2003 Events July 2007 January 2009 January 2009 Is global warming slowing down? Arctic Sea Ice Climatesafety.org climatesafety.org
More informationReferenced Abstracts/Proceedings from Presentations at Conferences
Referenced Abstracts/Proceedings from Presentations at Conferences 1. (2016) Kulmala M., H.K. Lappalainen, T. Petäjä, V.M. Kerminen, R. Makkonen, P.Alekseychik, N. Zaitseva, J. Kujansuu, A. Scherbinin,
More informationTreatment of Land-Use and Urbanization
Treatment of Land-Use and Urbanization LECTURE 9 Alexander Mahura Danish Meteorological Institute, DMI, Copenhagen, Denmark NetFAM Summer School on Integrated Modelling 7-12 July 2008, Zelenogorsk, Russia
More informationNordic weather extremes as simulated by the Rossby Centre Regional Climate Model: model evaluation and future projections
Nordic weather extremes as simulated by the Rossby Centre Regional Climate Model: model evaluation and future projections Grigory Nikulin, Erik Kjellström, Ulf Hansson, Gustav Strandberg and Anders Ullerstig
More informationApplication and verification of ECMWF products 2009
Application and verification of ECMWF products 2009 Danish Meteorological Institute Author: Søren E. Olufsen, Deputy Director of Forecasting Services Department and Erik Hansen, forecaster M.Sc. 1. Summary
More informationDO WE NEED URBAN PARAMETERIZATION IN HIGH RESOLUTION SIMULATIONS?
Charles University Faculty of Mathematics and Physics Dept. of Atmospheric Physics V Holešovičkách 2, Prague Czech Republic DO WE NEED URBAN PARAMETERIZATION IN HIGH RESOLUTION SIMULATIONS? Tomáš Halenka,
More informationWhat is Climate? Understanding and predicting climatic changes are the basic goals of climatology.
What is Climate? Understanding and predicting climatic changes are the basic goals of climatology. Climatology is the study of Earth s climate and the factors that affect past, present, and future climatic
More informationMESOSCALE MODELLING OVER AREAS CONTAINING HEAT ISLANDS. Marke Hongisto Finnish Meteorological Institute, P.O.Box 503, Helsinki
MESOSCALE MODELLING OVER AREAS CONTAINING HEAT ISLANDS Marke Hongisto Finnish Meteorological Institute, P.O.Box 503, 00101 Helsinki INTRODUCTION Urban heat islands have been suspected as being partially
More informationData assimilation and inverse problems. J. Vira, M. Sofiev
Data assimilation and inverse problems J. Vira, M. Sofiev SILAM winter school, 2013 Introduction How to combine observations and model fields into an estimate of the atmospheric state? Chemical data assimilation
More informationUrban heat island in the metropolitan area of São Paulo and the influence of warm and dry air masses during summer
Urban heat island in the metropolitan area of São Paulo and the influence of warm and dry air masses during summer Flavia N. D. Ribeiro1, Arissa S. umezaki1, Jhonathan F. T. de Souza1, Jacyra Soares2,
More informationAppendix 1: UK climate projections
Appendix 1: UK climate projections The UK Climate Projections 2009 provide the most up-to-date estimates of how the climate may change over the next 100 years. They are an invaluable source of information
More informationCLIPDAR -- DESIGN GUIDELINE FOR A CLIMATE PROJECTION DATA BASE AND SPECIFIC CLIMATE
CEDR Transnational Road Research Programme Call 2012 Road owners adapting to Climate Change CLIPDAR -- DESIGN GUIDELINE FOR A CLIMATE PROJECTION DATA BASE AND SPECIFIC CLIMATE INDICES FOR ROADS CHRISTOPH
More informationClimate Downscaling 201
Climate Downscaling 201 (with applications to Florida Precipitation) Michael E. Mann Departments of Meteorology & Geosciences; Earth & Environmental Systems Institute Penn State University USGS-FAU Precipitation
More informationSeamless weather and climate for security planning
Seamless weather and climate for security planning Kirsty Lewis, Principal Climate Change Consultant, Met Office Hadley Centre 28 June 2010 Global Climate Models Mitigation timescale changes could be avoided
More informationMesoscale meteorological models. Claire L. Vincent, Caroline Draxl and Joakim R. Nielsen
Mesoscale meteorological models Claire L. Vincent, Caroline Draxl and Joakim R. Nielsen Outline Mesoscale and synoptic scale meteorology Meteorological models Dynamics Parametrizations and interactions
More informationRoad Weather Modelling System: Verification for Road Weather Season
Road Weather Modelling System: Verification for 2010-2011 Road Weather Season Claus Petersen, Alexander Mahura, Bent Sass Copenhagen 2011 www.dmi.dk/dmi/tr11-19.pdf page 1 of 28 Colophon Serial title:
More informationTendencias y proyecciones futuras de tormentas y vientos extremos
(CSIC-UC) Tendencias y proyecciones futuras de tormentas y vientos extremos Prof. Jose Manuel Gutiérrez Instituto de Física de Cantabria (CSIC - Universidad de Cantabria) gutierjm@unican.es Proyecciones
More informationAtmosphere and Weather Revision Notes
Atmosphere and Weather Revision Notes Atmosphere The blanket of gases that surrounds the Earth is called the atmosphere. The main gases are nitrogen (78 %), oxygen (21 %), water vapour, ozone and carbon
More informationGEOGRAPHY EYA NOTES. Weather. atmosphere. Weather and climate
GEOGRAPHY EYA NOTES Weather and climate Weather The condition of the atmosphere at a specific place over a relatively short period of time Climate The atmospheric conditions of a specific place over a
More informationThe benefits and developments in ensemble wind forecasting
The benefits and developments in ensemble wind forecasting Erik Andersson Slide 1 ECMWF European Centre for Medium-Range Weather Forecasts Slide 1 ECMWF s global forecasting system High resolution forecast
More informationRR#5 - Free Response
Base your answers to questions 1 through 3 on the data table below and on your knowledge of Earth Science. The table shows the area, in million square kilometers, of the Arctic Ocean covered by ice from
More informationNew applications using real-time observations and ECMWF model data
New applications using real-time observations and ECMWF model data 12 th Workshop on Meteorological Operational Systems Wim van den Berg [senior meteorological researcher, project coordinator] Overview
More informationClimate Dynamics (PCC 587): Hydrologic Cycle and Global Warming
Climate Dynamics (PCC 587): Hydrologic Cycle and Global Warming D A R G A N M. W. F R I E R S O N U N I V E R S I T Y O F W A S H I N G T O N, D E P A R T M E N T O F A T M O S P H E R I C S C I E N C
More informationClaus Petersen* and Bent H. Sass* Danish Meteorological Institute Copenhagen, Denmark
6.8 Improving of road weather forecasting by using high resolution satellite data Claus Petersen* and Bent H. Sass* Danish Meteorological Institute Copenhagen, Denmark. INTRODUCTION Observations of high
More information4.3 Climate (6.3.3) Explore this Phenomena. The same sun shines on the entire Earth. Explain why these two areas have such different climates.
Explore this Phenomena The same sun shines on the entire Earth. 4.3 Climate (6.3.3) Explain why these two areas have such different climates. 89 6.3.3 Climate Develop and use a model to show how unequal
More informationAreas of the World with high Insolation
Areas of the World with high Insolation 22 /43 Africa Annual Average Global Horizontal Solar Radiation Map 19 Jul 2006 A map depicting model estimates of monthly average daily total radiation using inputs
More informationLecture 4 Air Temperature. Measuring Temperature. Measuring Temperature. Surface & Air Temperature. Environmental Contrasts 3/27/2012
Lecture 4 Air Temperature Geo210 An Introduction to Physical Geography Temperature Concepts and Measurement Temperature the average kinetic energy (motion) of molecules of matter Temperature Scales Fahrenheit
More information1990 Intergovernmental Panel on Climate Change Impacts Assessment
1990 Intergovernmental Panel on Climate Change Impacts Assessment Although the variability of weather and associated shifts in the frequency and magnitude of climate events were not available from the
More informationClimate services in support of the energy transformation
services in support of the energy transformation EGU 11 April 2018, Vienna, Austria Climate Alberto Troccoli, Sylvie Parey, and the C3S ECEM team O u t l i n e Background of the C3S European Climatic Energy
More informationAtmospheric patterns for heavy rain events in the Balearic Islands
Adv. Geosci., 12, 27 32, 2007 Author(s) 2007. This work is licensed under a Creative Commons License. Advances in Geosciences Atmospheric patterns for heavy rain events in the Balearic Islands A. Lana,
More informationWhy There Is Weather?
Lecture 6: Weather, Music Of Our Sphere Weather and Climate WEATHER The daily fluctuations in atmospheric conditions. The atmosphere on its own can produce weather. (From Understanding Weather & Climate)
More information3A: Use a model to describe how the flow of energy from the sun influences weather patterns and interacts with the layers of the atmosphere
3A: Use a model to describe how the flow of energy from the sun influences weather patterns and interacts with the layers of the atmosphere 1. Shade in the layers of the atmosphere red if the temperature
More informationAPPLICATIONS OF DOWNSCALING: HYDROLOGY AND WATER RESOURCES EXAMPLES
APPLICATIONS OF DOWNSCALING: HYDROLOGY AND WATER RESOURCES EXAMPLES Dennis P. Lettenmaier Department of Civil and Environmental Engineering For presentation at Workshop on Regional Climate Research NCAR
More informationChapter 7 Properties of the Atmosphere
14. Day Breezes H L Chapter 7 Properties of the Atmosphere Questions Pages 177 179 1. (3) 2. (4) 3. (4) 4. (3) 5. (2) 6. (3) 7. (2) 8. (2) 9. (3) 10. (1) 11. (4) 12. (2) Questions Pages 186 188 13. (3)
More informationGlobal warming and Extremes of Weather. Prof. Richard Allan, Department of Meteorology University of Reading
Global warming and Extremes of Weather Prof. Richard Allan, Department of Meteorology University of Reading Extreme weather climate change Recent extreme weather focusses debate on climate change Can we
More information2016 Meteorology Summary
2016 Meteorology Summary New Jersey Department of Environmental Protection AIR POLLUTION AND METEOROLOGY Meteorology plays an important role in the distribution of pollution throughout the troposphere,
More informationClimate Change and Runoff Statistics in the Rhine Basin: A Process Study with a Coupled Climate-Runoff Model
IACETH Climate Change and Runoff Statistics in the Rhine Basin: A Process Study with a Coupled Climate-Runoff Model Jan KLEINN, Christoph Frei, Joachim Gurtz, Pier Luigi Vidale, and Christoph Schär Institute
More informationS e a s o n a l F o r e c a s t i n g f o r t h e E u r o p e a n e n e r g y s e c t o r
S e a s o n a l F o r e c a s t i n g f o r t h e E u r o p e a n e n e r g y s e c t o r C3S European Climatic Energy Mixes (ECEM) Webinar 18 th Oct 2017 Philip Bett, Met Office Hadley Centre S e a s
More informationTHE EARTH S CLIMATE SYSTEM
THE EARTH S CLIMATE SYSTEM Earth s Climate System is driven by interactions between the parts of our biosphere So.what is the Biosphere? a relatively thin layer of Earth that has conditions suitable for
More informationPresentation Overview. Southwestern Climate: Past, present and future. Global Energy Balance. What is climate?
Southwestern Climate: Past, present and future Mike Crimmins Climate Science Extension Specialist Dept. of Soil, Water, & Env. Science & Arizona Cooperative Extension The University of Arizona Presentation
More informationScience 1206 Chapter 1 - Inquiring about Weather
Science 1206 Chapter 1 - Inquiring about Weather 1.1 - The Atmosphere: Energy Transfer and Properties (pp. 10-25) Weather and the Atmosphere weather the physical conditions of the atmosphere at a specific
More informationLarge Scale Weather Patterns Associated with California Heat Waves and their use in a Hindcast and Future Climate
Large Scale Weather Patterns Associated with California Heat Waves and their use in a Hindcast and Future Climate Richard Grotjahn Atmospheric Science Program Dept. of LAWR, UCD, Davis, CA, USA Outline
More informationp = ρrt p = ρr d = T( q v ) dp dz = ρg
Chapter 1: Properties of the Atmosphere What are the major chemical components of the atmosphere? Atmospheric Layers and their major characteristics: Troposphere, Stratosphere Mesosphere, Thermosphere
More informationRe-analysis activities at SMHI
Re-analysis activities at SMHI by: Anna Jansson and Per Kållberg Contents Variational data assimilation at SMHI Operational MESAN Applications of MESAN MESAN used for a long time period Variational data
More informationClimate Modeling and Downscaling
Climate Modeling and Downscaling Types of climate-change experiments: a preview 1) What-if sensitivity experiments increase the optically active gases and aerosols according to an assumed scenario, and
More informationFuture climate change in the Antilles: Regional climate, tropical cyclones and sea states
Future climate change in the Antilles: Regional climate, tropical cyclones and sea states Ali Belmadani Météo-France Antilles-Guiana (DIRAG), Martinique Acknowledgements: P. Palany, R. Pilon, F. Chauvin,
More informationContents. Section 1: Climate Factors. Section 2: Climate Types. Section 3: Climate Effects
Contents Section 1: Climate Factors 1. Weather or Climate?.... 2 2. Elements of Climate.... 4 3. Factors Affecting Climate.... 10 4. Comparing Climates.... 15 5. Quiz 1.... 20 Section 2: Climate Types
More informationToward the new CH2018 climate scenarios for Switzerland
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Toward the new CH2018 climate scenarios for Switzerland Andreas Fischer, Abteilung Klima, MeteoSchweiz Elias
More informationProjections of future climate change
Projections of future climate change Matthew Collins 1,2 and Catherine A. Senior 2 1 Centre for Global Atmospheric Modelling, Department of Meteorology, University of Reading 2 Met Office Hadley Centre,
More informationChapter outline. Reference 12/13/2016
Chapter 2. observation CC EST 5103 Climate Change Science Rezaul Karim Environmental Science & Technology Jessore University of science & Technology Chapter outline Temperature in the instrumental record
More informationObserved Climate Variability and Change: Evidence and Issues Related to Uncertainty
Observed Climate Variability and Change: Evidence and Issues Related to Uncertainty David R. Easterling National Climatic Data Center Asheville, North Carolina Overview Some examples of observed climate
More information6.13 SYSTEMATIC ANALYSIS OF METEOROLOGICAL CONDITIONS CAUSING SEVERE URBAN AIR POLLUTION EPISODES IN THE CENTRAL PO VALLEY
6.13 SYSTEMATIC ANALYSIS OF METEOROLOGICAL CONDITIONS CAUSING SEVERE URBAN AIR POLLUTION EPISODES IN THE CENTRAL PO VALLEY Sandro Finardi 1, and Umberto Pellegrini 2 1 ARIANET, via Gilino 9, 2128 Milano,
More informationClimate. Annual Temperature (Last 30 Years) January Temperature. July Temperature. Average Precipitation (Last 30 Years)
Climate Annual Temperature (Last 30 Years) Average Annual High Temp. (F)70, (C)21 Average Annual Low Temp. (F)43, (C)6 January Temperature Average January High Temp. (F)48, (C)9 Average January Low Temp.
More informationExtremely cold weather events caused by arctic air mass and its synoptic situation in Finland from the year 1950 onwards
Extremely cold weather events caused by arctic air mass and its synoptic situation in Finland from the year 1950 onwards Senior meteorologist Henri Nyman Finnish Meteorological Institute, Weather and Safety
More informationA downscaling and adjustment method for climate projections in mountainous regions
A downscaling and adjustment method for climate projections in mountainous regions applicable to energy balance land surface models D. Verfaillie, M. Déqué, S. Morin, M. Lafaysse Météo-France CNRS, CNRM
More informationApplication and verification of the ECMWF products Report 2007
Application and verification of the ECMWF products Report 2007 National Meteorological Administration Romania 1. Summary of major highlights The medium range forecast activity within the National Meteorological
More informationWind: Global Systems Chapter 10
Wind: Global Systems Chapter 10 General Circulation of the Atmosphere General circulation of the atmosphere describes average wind patterns and is useful for understanding climate Over the earth, incoming
More informationClimate versus Weather
Climate versus Weather What is climate? Climate is the average weather usually taken over a 30-year time period for a particular region and time period. Climate is not the same as weather, but rather,
More informationAS Atmospheric Sciences Orals and PICOs Monday, 08 April
AS Atmospheric Sciences Orals and PICOs Monday, 08 April MO1, 08:30 10:00 MO2, 10:30 12:00 MOL, 12:15 13:15 MO3, 13:30 15:00 AS1.1, Numerical weather prediction, data assimilation and ensemble forecasting,
More informationURBAN HEAT ISLAND IN SEOUL
URBAN HEAT ISLAND IN SEOUL Jong-Jin Baik *, Yeon-Hee Kim ** *Seoul National University; ** Meteorological Research Institute/KMA, Korea Abstract The spatial and temporal structure of the urban heat island
More informationThe 21st century decline in damaging European windstorms David Stephenson & Laura Dawkins Exeter Climate Systems
The 21st century decline in damaging European windstorms David Stephenson & Laura Dawkins Exeter Climate Systems Acknowledgements: Julia Lockwood, Paul Maisey 6 th European Windstorm workshop, Reading,
More informationThermal / Solar. When air is warmed it... Rises. Solar Energy. Evaporation. Condensation Forms Clouds
Thermal / Solar Light from the Sun is transformed into what type of energy when it hits Earth's surface? Rises When air is warmed it... Solar Energy Water moves through the water cycle using what type
More informationMeteorology Practice Test
Meteorology Practice Test 1. Transition zones between two air masses of different densities are called what? 2. A front occurs when a cold air mass replaces a warmer one. 3. A front occurs when a warm
More informationClimate Change or Climate Variability?
Climate Change or Climate Variability? Key Concepts: Greenhouse Gas Climate Climate change Climate variability Climate zones Precipitation Temperature Water cycle Weather WHAT YOU WILL LEARN 1. You will
More informationForecasting Local Weather
Forecasting Local Weather Sea/Land Breeze Temperature Dew Fog Frost Snow Thunderstorms Tropical Cyclones Temperatures: Radiation Balance Typical Diurnal Variation of Temperature Min soon after dawn Temp
More informationAtmospheric Circulation
Atmospheric Circulation Introductory Oceanography Instructor: Ray Rector Atmospheric Circulation Key Topics Composition and Structure Solar Heating and Convection The Coriolis Effect Global Wind Patterns
More informationESCI 344 Tropical Meteorology Lesson 7 Temperature, Clouds, and Rain
ESCI 344 Tropical Meteorology Lesson 7 Temperature, Clouds, and Rain References: Forecaster s Guide to Tropical Meteorology (updated), Ramage Tropical Climatology, McGregor and Nieuwolt Climate and Weather
More informationA re-sampling based weather generator
A re-sampling based weather generator Sara Martino 1 Joint work with T. Nipen 2 and C. Lussana 2 1 Sintef Energy Resources 2 Norwegian Metereologic Institute Stockholm 7th Dec. 2017 Sara Martino Joint
More informationSocial Studies. Chapter 2 Canada s Physical Landscape
Social Studies Chapter 2 Canada s Physical Landscape Introduction Canada s geography its landforms and climate - has a great impact on Canadians sense of identity. Planet Earth The earth is divided into
More informationApplication and verification of ECMWF products 2009
Application and verification of ECMWF products 2009 Hungarian Meteorological Service 1. Summary of major highlights The objective verification of ECMWF forecasts have been continued on all the time ranges
More informationWeather & Climate of Virginia
Weather & Climate of Virginia Robert E. Davis Professor of Climatology Dept. of Environmental Sciences University of Virginia Email: red3u@virginia.edu Rivanna Master Naturalists March 14, 2017 Arctic
More informationStrategy for Urbanization of Different Types of Models
Chapter 3. Strategy for Urbanization of Different Types of Models 3.1 FUMAPEX Experience of Model Urbanisation Alexander Baklanov and FUMAPEX Team Danish Meteorological Institute, DMI, Copenhagen, Denmark
More informationClimate Variables for Energy: WP2
Climate Variables for Energy: WP2 Phil Jones CRU, UEA, Norwich, UK Within ECEM, WP2 provides climate data for numerous variables to feed into WP3, where ESCIIs will be used to produce energy-relevant series
More informationRegional climate modelling in the future. Ralf Döscher, SMHI, Sweden
Regional climate modelling in the future Ralf Döscher, SMHI, Sweden The chain Global H E H E C ( m 3/s ) Regional downscaling 120 adam 3 C HAM 4 adam 3 C HAM 4 trl A2 A2 B2 B2 80 40 0 J F M A M J J A S
More information